000 AXPZ20 KNHC 050226 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 0405 UTC SAT SEP 05 2009 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 0000 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0300 UTC. ...THE ITCZ... THE AXIS EXTENDS FROM 09N78W TO 09N100W TO 12N113W...THE ITCZ CONTINUES AGAIN FROM 10N120W TO 11N140W. SCATTERED MODERATE WITHIN 120 NM S OF AXIS E OF 88W. ...DISCUSSION... THE REMNANTS OF JIMENA ARE LOCATED OVER CENTRAL BAJA CALIFORNIA NEAR 27N112W AS A WEAK 1007 MB LOW. WHILE DEEP CONVECTION ENDED SEVERAL HOURS AGO...SIGNIFICANT LOW TOPPED SHOWERS ARE STILL OCCURRING...ESPECIALLY WHERE ENHANCED BY UPSLOPE FLOW. ADDITIONALLY...SEAS UP TO 8 FT MAY STILL BE OBSERVED IN THE CENTRAL GULF OF CALIFORNIA. THE REMNANTS FROM JIMENA SHOULD DISSIPATE WITHIN THE NEXT 24 HOURS. A BROAD AREA OF LOW PRESSURE IS CENTERED NEAR 13N115W...MOVING WNW ABOUT 12 KT. DEEP CONVECTION HAS INCREASED SOME WITH THIS SYSTEM DURING THE LAST FEW HOURS...BUT IS DISPLACED WELL NORTHWEST OF THE CENTER. MODERATE TO STRONG NORTHERLY WINDS ALOFT MAY SLOW ANY FURTHER DEVELOPMENT DURING THE NEXT COUPLE OF DAYS. THERE IS A LOW...LESS THAN 30 PERCENT...CHANCE OF TROPICAL CYCLONE FORMATION IN THE NEXT 48 HOURS. THE REMNANT LOW FROM KEVIN IS STILL FOUND NEAR 18N125W... DRIFTING SLOWLY SW. NO DEEP CONVECTION IS ASSOCIATED WITH THIS SYSTEM...THOUGH A WELL DEFINED VORTEX REMAINS VISIBLE IN THE LOWER CLOUDS. THIS LOW SHOULD DISSIPATE WITHIN THE NEXT 24 HOURS. A MODEST INCREASE IN THE TRADEWINDS IN THE WESTERNMOST PORTION OF OUR DOMAIN BETWEEN 15N AND 23N IS EXPECTED IN ABOUT 48 HOURS...LEADING TO SOME 20 KT WINDS AND SEAS TO 8 FT. A WEAK PAPAGAYO WIND EVENT WEST OF NICARAGUA HAD PREVIOUSLY BEEN IN THE HIGH SEAS FORECAST. WHILE THIS MAY BRIEFLY REACH INTO THE 20 KT WIND RANGE THRESHOLD IN THE NEXT TWO MORNINGS...THE WINDS IN GENERAL SHOULD BE EASTERLY 10 TO 15 KT. NO SIGNIFICANT SWELL IS PROPAGATING INTO OUR REGION AT THIS TIME OR IN THE NEXT 48 HOURS. $$ CWL